Fractional derivative modelling for rheological consolidation of multilayered soil under time-dependent loadings and continuous permeable boundary conditions

被引:14
|
作者
Ding, Pan [1 ]
Xu, Riqing [1 ,2 ,3 ]
Zhu, Yihong [1 ]
Wen, Minjie [1 ]
机构
[1] Zhejiang Univ, Res Ctr Coastal & Urban Geotech Engn, Hangzhou 310058, Peoples R China
[2] Engn Res Ctr Urban Underground Space Dev Zhejiang, Hangzhou 310058, Peoples R China
[3] Zhejiang California Int Nano Syst Inst, Taizhou Branch, Taizhou 318000, Peoples R China
基金
中国国家自然科学基金;
关键词
Continuous drainage boundary; Fractional derivative Merchant model; Laplace transform; Multilayered soil; Rheological consolidation; Time-dependent loadings; ONE-DIMENSIONAL CONSOLIDATION; NUMERICAL INVERSION; CONSTITUTIVE MODEL; LAYERED SOILS; BEHAVIOR;
D O I
10.1007/s11440-021-01417-0
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
This paper investigates the one-dimensional rheological consolidation problem of multilayered soils subjected to different time-dependent loadings and continuous permeable boundary conditions. First, by introducing fractional calculus, the conventional Merchant constitutive model is modified to the fractional derivative Merchant (FDM) model, and the newly established model is introduced to describe the rheological characteristics of soil. Subsequently, to simplify the solving process of the consolidation equation, the Laplace transform is utilized to convert the partial differential equations into ordinary differential equations, and the analytical solutions in the Laplace domain are obtained. Furthermore, the solutions in the time domain are obtained by using Abate's fixed Talbot method (AFT method), which is one of the numerical Laplace inversion methods, and the corresponding computer program for the AFT method is attached. A comparison between the degenerated results of this study and those in the literature suggests that the present solutions are more general and applicable. Finally, several instances are provided to study the impacts of model parameters on the consolidation phenomenon.
引用
收藏
页码:2287 / 2304
页数:18
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